地壳厚度对中国金矿床空间分布规律的制约
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摘要
圈定成矿远景区并进行矿产勘查,是新一轮找矿突破的重要内容。在当前大数据和深部地球的背景下,文章根据金矿床空间分布对所在的地壳厚度和地表高程进行了空间连接和相关统计分析,并初步圈定了金矿床的成矿远景区。研究结果表明,地壳厚度为35 km和高程为200 m左右的区域,是金矿床产出的有利区域,并且金矿床的地壳厚度极值和频率呈现分形关系,为金矿床靶区的预测,提供了基本的非线性深部矿产资源预测数学模型;根据金矿床和地壳厚度、高程等的关系,对金矿床的优势成矿远景区进行了预测。预测结果显示,松嫩盆地周边,济南-郑州-武汉-长沙-南宁沿线及周边,是金矿床产出的有利远景区域。
The area which is defined as metallogenic potential area and requires following up in mineral exploration plays an important role in the process of prospecting breakthrough and deposit study. Based on the background of big data and deep earth, this paper analyzes the correlation statistics between crust thickness, elevation and gold deposits, and preliminarily delineates the metallogenic prospective area of the gold deposits. The results show that the area with ca. 35 km in crust thickness and ca. 200 m in height is a favorable area for gold mineralization.In addition, the fractal relation between the extreme value of the crust thickness and the frequency of the gold deposit provides a basic non-linear prediction model for gold deposit. According to the correlation between gold deposits, crustal thickness and elevation, the metallogenic prospective area of gold deposit is predicted. The prediction results show that the Ji'nan-Zhengzhou-Wuhan-Changsha-Nanning region along the periphery of Songnen basin is a favorable prospective area for gold mineralization.
The area which is defined as metallogenic potential area and requires following up in mineral exploration plays an important role in the process of prospecting breakthrough and deposit study. Based on the background of big data and deep earth, this paper analyzes the correlation statistics between crust thickness, elevation and gold deposits, and preliminarily delineates the metallogenic prospective area of the gold deposits. The results show that the area with ca. 35 km in crust thickness and ca. 200 m in height is a favorable area for gold mineralization.In addition, the fractal relation between the extreme value of the crust thickness and the frequency of the gold deposit provides a basic non-linear prediction model for gold deposit. According to the correlation between gold deposits, crustal thickness and elevation, the metallogenic prospective area of gold deposit is predicted. The prediction results show that the Ji'nan-Zhengzhou-Wuhan-Changsha-Nanning region along the periphery of Songnen basin is a favorable prospective area for gold mineralization.
引文
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Li T D.2010.Principal characteristics of the lithosphere of China[J].Earth Science Frontiers,1(1):45-56.
Liu X Y,Zhang Q and Zhang C L.2017.A discussion on the tectonic setting of global Cenozoic andesite[J].Chinese Journal of Geology,52(3):649-667(in Chinese with English abstract).
Liu X L,Li W C,Zhang N,Zhu J,Luo Y,Yang F C,Zhang C Z and Wang S S.2017.Comparative study on mineralization related granite of Pulang porphyry copper deposit in northwestern Yunnan and global adakite:The preliminary result of big data research[J].Acta Petrological Sinica,34(2):289-302(in Chinese with English abstract).
Maier W D and Groves D I.2011.Temporal and spatial controls on the formation of magmatic PGE and Ni-Cu deposits[J].Mineralium Deposita,46:841-857.
Mandelbrot B B,Passoja D E and Paullay A J.1984.Fractal character of fracture surfaces of metal[J].Nature,308(5961):721-722.
Mcdonough W F 2003.Compositional model for the earth's core[J].Treatise on Geochemistry,2:547-568.
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Richards J P.2009.Postsubduction porphyry Cu-Au and epithermal Au deposits:Products of remelting of subduction-modified lithosphere[J].Geology,37(3):247-250.
Richards J P.2011.Magmatic to hydrothermal metal fluxes in convergent and collided margins[J].Ore Geology Reviews,40(1):1-26.
Ruiz C R,Corominas J and Mavrouli O.2017.A fractal fragmentation model for rockfalls[J].Landslides,14:875-889.
Shen W.2008.Fractal analysis of the temporal-spatial distribution of Cretaceous mineral deposit in China[J].Journal of Geomechanics,14(1):57-64(in Chinese with English abstract).
Sim B L,Agterberg F P and Beaudry C.1999.Determining the cutoff between background and relative base metal smelter contamination levels using multifractal methods[J].Computers&Geosciences,25(9):1023-1041.
Solomon M.1990.Subduction,arc reverasal,and the origin of porphyry copper-gold deposit in island arcs[J].Geology,18(6):630-633.
Sun T and Liu L M.2014.Delineating the complexity of Cu-Mo mineralization in a porphyry intrusion by computational and fractal modeling:A case study of the Chehugou deposit in the Chifeng district,Inner Mongolia[J].China Journal of Geochemical Exploration,144:128-143.
Sun Y J,Dong S W,Zhang H,Han L and Shi Y L.2013.3D thermal structure of the continental lithosphere beneath China and adjacent regions[J].Journal of Asian Earth Sciences,62(5):697-704.
Tan Y J,Wen M,Zhu Y Q and Qu H G.2017.Research on the big data characteristics[J].China Mining Magazine,26(9):67-71(in Chinese with English abstract).
Teng J W,Zhang Z J,Zhang X K,Wang C Y,Gao R,Yang B J,Qiao YH and Deng Y F.2013.Investigation of the Moho discontinuity beneath the Chinese mainland using deep seismic sounding profiles[J].Tectonophysics,609:202-216.
Teng J W,Deng Y F,Badal J and Zhan Y Q.2014.Moho depth,seismicity and seismogenic structure in China mainland[J].Tectonophysics,627:108-121.
Wang C M,Deng J,Bagas L and Wang Q.2017.Zircon Hf-isotopic mapping for understanding crustal architecture and metallogenesis in the Eastern Qinling Orogen[J].Gondwana Research,50:293-310.
Wang J R,Chen W F,Zhang Q,Jin W J,Jiao S T,Wang Y X,Yang Jand Pan Z J.2017.MORB data mining:reflection of basalt discrimination diagram[J].Geotectonica et Metallogenica,41(2):420-431(in Chinese with English abstract).
Wang Q L.1989.The ancient crust of the Precambrian is the basis for the gold deposits[J].Geology and Prospecting,8(8):38(in Chinese with English abstract).
Wu C L,Liu G,Zhang X L,He Z W and Zhang Z T.2016.Discussion on geological science big data and its applications[J].Chinese Science Bulletin,61(16):1797-1807(in Chinese with English abstract).
Yang M G,Huang S B,Lou F S,Tang W X and Mao S B.2009.Lithospheric structure and large-scale metallogenic process in Southeast China[J].Geology in China,36(3):528-543(in Chinese with English abstract).
Yang Q D.2014.Variation of Nd isotopic compositions in the granitoids from the Great Xing’an Mountains and adjacent areas:Implications for architecture and growth of continental crust[D].Supervisor:Wang T.Beijing:Chinese Academy of Geological Science,1-219(in Chinese with English abstract).
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